STUDY ON REDUCTION MECHANISM OF WAVE PRESSURE AT LANDWARD SIDE OF CAISSON DUE TO TSUNAMI OVERFLOW

Bibliographic Information

Other Title
  • 津波の越流による混成堤ケーソン岸側での水圧の低下機構に関する研究

Abstract

 The mechanism of a decrease in wave pressure at the landward side of a caisson on a rubble mound during tsunami overflow is investigated using a coupled fluid-structure interaction model. Numerical results show that the wave pressure acting on the landward surface of the caisson after the onset of the overflow is overestimated by the hydrostatic pressure calculated from an elevation in the water surface. This discrepancy is caused by vortices formed by the separation of the flow. Furthermore, a temporal decrease in the wave pressure results from an increase in the flow velocity. Based on the numerical results, an approximation equation is proposed to predict the reduction rate of the wave force acting on the landward surface of the caisson from water surface elevations at the seaward and landward sides of the caisson.

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Details 詳細情報について

  • CRID
    1390001205352546688
  • NII Article ID
    130004961748
  • DOI
    10.2208/jscejoe.69.i_389
  • ISSN
    21854688
  • Text Lang
    ja
  • Data Source
    • JaLC
    • Crossref
    • CiNii Articles
    • KAKEN
  • Abstract License Flag
    Disallowed

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